Year‐Round δ¹³C‐CH₄ Reveals Seasonal Transition in Methane‐Related Processes in a Boreal Mire

While boreal mires are known to be a significant natural source of methane (CH 4 ), the seasonality of the related processes and their controls are still poorly understood. Here we aim to characterize CH 4 production, oxidation and transport, and their drivers in a boreal mire using year‐round continuous measurements of stable carbon isotope composition (δ 13 C‐CH 4 ) in dissolved and emitted CH 4 . We found reversed vertical profiles of δ 13 C‐CH 4 in the summer (higher values at surface) and in the winter (higher values at bottom). The 13 C enriched emitted CH 4 , as compared to pore water CH 4 , indicated methane oxidation at the peat‐snow interface by sphagnum mosses in the winter. The observed hysteretic δ 13 C‐CH 4 ‐ pCH 4 relation indicated the importance of substrate availability for methane production in addition to soil temperature, and their time‐lagged seasonal cycles. Our data also demonstrated the dominance of plant‐mediated transport in the summer, the dominance of diffusion through peat and moss matrix (with associated microbial methane oxidation) in the winter and a transition in the spring and autumn. In general, the measured δ 13 C values of emitted CH 4 at this and other northern mires are considerably lower than the values used in atmospheric inversion models. Our comprehensive data set provided invaluable insight into wetland δ 13 C‐CH 4 , the dynamic interplay of multiple processes related to CH 4 emission in boreal mires, especially in the rarely studied winter, spring, and autumn, the incorporation of which into Earth System Models will allow more accurate prediction of wetland responses to ongoing climate change.